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1
Read before the Association at Atlantic City, New Jersey, April 25, 1960. Manuscript received, January 1, 1960.
2
Department of Geology, University of Utah. The following paper is a summary of observations of many individual geologists who have taken part in the intensified study of the Colorado Plateau during recent years. Only by drawing freely upon the work of others is it possible to present a fair and comprehensive summary of what is known about the continental sandstone bodies of this region.

Abstract

The Colorado Plateau has been the site of accumulation and preservation of nonmarine sediments since late Paleozoic time. The climatic conditions have been desert-like for long periods, and wind-blown sand is a common sedimentary type. Much of the alluvial material was carried only relatively short distances and can be related to nearby source areas. The deep and intricate erosion of the region permits excellent three-dimensional views of the sedimentary bodies.

Extensive eolian deposits occur in the Permian, Triassic, and Jurassic Systems. These are mainly interpreted as superposed dune fields. In many instances the edges of the formations are abrupt, and comparison with modern sharply defined dune areas is obvious. Tangential cross-bedding with occasional contorted masses characterize these deposits. Chief interest attaches to the determination of wind directions; apparently the source of most of the,sand lay to the north and northwest.

Fluvial deposits are common above the Pennsylvanian. These offer excellent opportunity to study sedimentary variations resulting from differences in climate, weathering, distance of transport, provenance, and energy relations of stream systems. The common occurrence of uranium deposits in the fluvial sandstones has stimulated geologic investigation. The petroleum possibilities of these beds are also receiving increased attention.

Practically every type of deposit seen in process of formation in modern rivers can be detected in the consolidated rocks. The overbank or flood-plain deposits are of less variety and interest than the channel deposits. All types of bars and channel-fill deposits are present, but those formed during the building of alluvial plains are most common. Apparently, the final composition of a typical fluvial formation depends on the gradient of the streams, the total amount of sediment supplied, and the relative amounts of fine and coarse material.

Internal structures of channel sandstones show great variety and can be related to stream volume and velocity. Ripple mark, festoon cross-bedding, rib and furrow, and lineation are the most common.

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